Influence of high temperature on the processes of formation of groundwater chemical composition during the interaction of carbonate rocks with water
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Abstract
One of the most important factors in the formation of the chemical composition of groundwater is high temperature, the influence of which affects the intensity of dissolution and hydrolysis of minerals, and cation exchange.
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References
- Kissin I.G., Pakhomov S.I. On the influence of high temperatures on the formation of the chemical composition of groundwater. - Geochemistry, 1967, No. 3.
- Kissin I.G., Pakhomov S.I. On the Possibility of Carbonic Acid Generation in the Subsurface at Moderately High Temperatures. - Reports of the USSR Academy of Sciences, 1967, vol. 174, № 2.
- Ovcharenko F.D. Hydrophilicity of clays and clay minerals. Kiev, Izd. of the Academy of Sciences of the Ukrainian SSR, 1961.
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